Climate change in the circum-North Atlantic region during the last deglaciation

Details Climate change in the circum-North Atlantic region during the last deglaciation Climate change in the circum-North Atlantic region during the last deglaciation

Apr 1989

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1989natur.338..553o&link_type=abstract

Nature (ISSN 0028-0836), vol. 338, April 13, 1989, p. 553-557. Research supported by NSF and NASA.

Astronomy and Astrophysics

Astronomy

35

Atlantic Ocean, Climate Change, Glaciers, Northern Hemisphere, Paleoclimatology, Atmospheric Pressure, Atmospheric Temperature, Caribbean Sea, Gulf Of Mexico, Land Ice, Sea Surface Temperature

Scientific paper

A survey of new and published palaeoclimate data indicates that both the high- and low-latitude North Atlantic regions were characterized by at least three synchronous periods of abrupt climate change during the last glacial-to-interglacial transition. Climate model results suggest that changes in the melting history of the Laurentide Ice Sheet may explain much of this nonlinear response of the climate system to astronomical (Milankovitch) forcing.

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